About: Britannia Guyots

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The Britannia Guyots (also known as Britannia Bank, Britannia Tablemount, Britannia Tablemounts, Brittania Guyots or Brittania Tablemounts) are a line of extinct volcanic seamounts in the Tasmantid Seamount Chain. The waters above it are incorporated in the Central Eastern Marine Park, an Australian marine park.

Attributes	Values
rdf:type	geo:SpatialThing
rdfs:label	Britannia Guyots (en)
rdfs:comment	The Britannia Guyots (also known as Britannia Bank, Britannia Tablemount, Britannia Tablemounts, Brittania Guyots or Brittania Tablemounts) are a line of extinct volcanic seamounts in the Tasmantid Seamount Chain. The waters above it are incorporated in the Central Eastern Marine Park, an Australian marine park. (en)
name	Britannia Guyots (en)
geo:lat	-28.283333 (xsd:float)
geo:long	155.640274 (xsd:float)
foaf:depiction
dcterms:subject	Miocene volcanoes Seamounts of the Tasman Sea Volcanoes of the Tasman Sea Guyots Hotspot volcanoes Polygenetic volcanoes
Wikipage page ID	71718266 (xsd:integer)
Wikipage revision ID	1109517864 (xsd:integer)
Link from a Wikipage to another Wikipage	Seamount Gold Coast, Queensland Miocene Australia Central Eastern Marine Park Miocene volcanoes Seamounts of the Tasman Sea Volcanoes of the Tasman Sea Tasmantid Seamount Chain Guyots Hotspot volcanoes Polygenetic volcanoes Australian marine parks Guyot
sameAs	Britannia Guyots Britannia Guyots
dbp:wikiPageUsesTemplate	dbt:Infobox_seamount dbt:Convert dbt:Coord dbt:Reflist dbt:Short_description
thumbnail	wiki-commons:Special:FilePath/Zealandia,_topographic_map.jpg?width=300
discovered	Named from the British cable ship "Britannia" (en)
group	Tasmantid Seamount Chain
location	To the east of the Gold Coast, Queensland, Australia (en)
map caption	Location of the Britannia Guyots (en)
map size	250 (xsd:integer)
pushpin map	Pacific Ocean (en)
type	Guyot
georss:point	-28.283333333333335 155.64027777777778
has abstract	The Britannia Guyots (also known as Britannia Bank, Britannia Tablemount, Britannia Tablemounts, Brittania Guyots or Brittania Tablemounts) are a line of extinct volcanic seamounts in the Tasmantid Seamount Chain. They are basaltic volcanoes that erupted between 17,600,000 and 20,800,000 years ago, with survey data that indicates they rise about 4,000 m (13,000 ft) above the local sea floor to a minimum depth of 421 m (1,381 ft). The sediments deposited on top of the alkali olivine basalt originate from the early Middle Miocene when the ocean water was tropical to subtropical. They were described as seamounts in 1961. The waters above it are incorporated in the Central Eastern Marine Park, an Australian marine park. (en)
prov:wasDerivedFrom	wikipedia-en:Britannia_Guyots?oldid=1109517864&ns=0
page length (characters) of wiki page	3714 (xsd:nonNegativeInteger)
foaf:isPrimaryTopicOf	wikipedia-en:Britannia_Guyots
geo:geometry	POINT(155.64027404785 -28.283332824707)
is Link from a Wikipage to another Wikipage of	Queensland Guyot Tasmantid Seamount Chain
is foaf:primaryTopic of	wikipedia-en:Britannia_Guyots

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